The Underground Water-Levels of The
342 WAITLEY ON UNDERGROUND WATER-LEVELS. [Selected (Paper No. 3228.) ‘‘ ‘I he Underground Water-Levels of the South Downs between Eastbourne and the River Cu~kmere.” By HENRYNICHELL WHITLEY, N. Inst. C.E. THE portion of the South Downs of Sussex referredto in the following Paper is the extremeeastern knoll, stretching from Eastbourne and Polegate on the east to the River Cuckmere on the west, and from theEnglish Channel on the south tothe Weald on the north, being about 5 miles in extent from east to west, and about 6 miles from north to south, Fig. 1. The hills rise considerably from the low land around, the highest portions being the eastern and northern escarpments, the ground having a steep slope towards the marshes and the Weald, and a more gradual one to the south and west. The district is bounded on the south by a lofty range of cliffs, of which Beachy Head is the highest part, being 536 feet above Ordnance datum. Northward from this point the escarpment varies between 500 feet and 600 feet, to Willingdon Hill, which has a height of 665 feet above Ordnance datum. Coomb Hill, at the north-east angle, is 638 feet, whilst Wilmington Hill, at the north-west end of the ridge, is 704 feet above Ordnance datum. The principal valley runs from that of the River Cuckmere by Westdean and Friston Place to Jevington Village, where there is a saddleback in the escarpment, about 290 feet above Ordnance datum; here it meets the deeply cut Wannock (or Filching) Glen, leading to the Weald.
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